- 7.2.1: What property allows O2 and CO2 to cross a lipid bilayer without th...
- 7.2.2: Why is a transport protein needed to move many water molecules rapi...
- 7.2.3: make connections Aquaporins exclude passage of hydronium ions (H3O+...
Solutions for Chapter 7.2: Membrane structure results in selective permeability
Full solutions for Campbell Biology | 10th Edition
A continuous spectrum with dark lines superimposed.
A high-pressure center characterized by a clockwise flow of air in the Northern Hemisphere.
The scientific study of the universe; it includes the observation and interpretation of celestial bodies and phenomena.
Sediment that is carried by a stream along the bottom of its channel.
The amount of heat required to raise the temperature of one gram of water 1° C.
A volcano composed of both lava flows and pyroclastic material.
The transfer of heat by the movement of a mass or substance. It can take place only in fluids.
A cone-shaped deposit at the base of the continental slope. The sediment is transported to the fan by turbidity currents that follow submarine canyons.
The point where a lens or mirror causes light rays to converge.
A general term referring to water vapor in the air but not to liquid droplets of fog, cloud, or rain.
A volcanic glass of felsic composition.
The relatively flat submerged zone that extends from the breaker line to the edge of the continental shelf.
Fog formed when rain evaporates as it falls through a layer of cool air.
An isolated volcanic peak that rises at least 1,000 meters (3,000 feet) above the deepocean floor.
A sudden and tremendous eruption in the solar chromosphere.
A narrow jet of rising material in the solar chromosphere.
The force per unit area acting on any surface within a solid.
Tropic of Capricorn
The parallel of latitude, 231?2 degrees south latitude, marking the southern limit of the Sun’s verticalrays.
A common term for a desert stream course that is typically dry except for brief periods immediately following a rain.
A seaward-facing cliff along a steep shoreline formed by wave erosion at its base and mass wasting